ATMOSPHERIC COMPOSITION CHANGE AT HIGH ELEVATIONS
Sandro Fuzzi
Institute of Atmospheric Sciences and Climate National Research Council Bologna, Italy
ATMOSPHERIC COMPOSITION CHANGE AT HIGH ELEVATIONS Sandro Fuzzi - - PowerPoint PPT Presentation
ATMOSPHERIC COMPOSITION CHANGE AT HIGH ELEVATIONS Sandro Fuzzi Institute of Atmospheric Sciences and Climate National Research Council Bologna, Italy Atmospheric change, Atmospheric change, environment, climate environment, climate
Institute of Atmospheric Sciences and Climate National Research Council Bologna, Italy
Changes in atmospheric composition induced by human activities directly affect many by human activities directly affect many environmental processes, determining environmental processes, determining climate, air quality and atmospheric inputs to climate, air quality and atmospheric inputs to ecosystems ecosystems
As a result of anthropogenic emissions, atmospheric composition changes affect the atmospheric composition changes affect the fundamental necessities for human existence: fundamental necessities for human existence: human health, food production, and human health, food production, and availability of water availability of water
energy production agriculture industry transportation farming deforestation
waste
Today, anthropogenic emissions Today, anthropogenic emissions
exceed by far natural sources exceed by far natural sources
Sulphur Emissions Northern Hemisphere
Nitrogen Fixation
pollution biomass burning
Koch et al., 2007 Koch et al., 2007
Mountains are marginal environments highly sensitive to global change sensitive to global change
At the same time, mountains provide unique
change processes and phenomena change processes and phenomena
At high mountain stations atmospheric background conditions and global change background conditions and global change processes can profitably be studied by means processes can profitably be studied by means
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10°42‘ E, 2165 m asl) is the highest peak of the Northern Apennines, the border line of two different climatic regions:
2 record in Europe
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MTC
SeaWIFFS SeaWIFFS satellite satellite
dust pollution aerosol Po Valley
(August 2007) (August 2007)
3 summer concentration
Polluted days Non - polluted days
NASA NASA-
MODIS/Terra
Pyramid Pyramid Observatory Observatory
Everest
/
/
34 5
Remote control
instrumentation is also possible Data are sent through satellite telecommunication
CNR-ISAC OPGC-CNRS DLR UNI-URB EV-K2-CNR UNEP – ABC mide pyra
PYRAMID
QA/QC
SHELTER CNR – ISAC Bologna
Formation of Formation of new particles new particles from precursor from precursor pollutants pollutants transported from transported from the valleys below the valleys below took place ca. took place ca. 40% of the days 40% of the days
16 months 16 months
Halocarbons are collected Halocarbons are collected in flasks in flasks on a weekly basis
and are then analysed for and are then analysed for 25 climatically relevant 25 climatically relevant species species
ABC ABC-
Pyramid
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è, F. Calzolari, , F. Calzolari,
Gobbi, P. Laj,
M. Maione, V. Mancinelli, Maione, V. Mancinelli, A. Marinoni, A. Petzold,
,
Roger, K. Sellegri, M. Sprenger, H. Venzac , GP. Verza, Verza,
CNR CNR -
Institute for Atmospheric Sciences and Climate, Bologna, Italy CNRS CNRS -
Université é Blaise Pascal, Aubi Blaise Pascal, Aubiè ère Cedex, France re Cedex, France Urbino University Urbino University -
Department of Environmental Sciences, Urbino, Italy DLR DLR – – Institute of Atmospheric Physics, Wessling, Germany Institute of Atmospheric Physics, Wessling, Germany ETHZ ETHZ -
Swiss Federal Institute of Technology, Zurich, Switzerland EV EV-
K2-
CNR Committee, Bergamo, Italy Committee, Bergamo, Italy